Microfossils in a specimen of Cambrian (?) sandstone from Karstula, Central Finland
Fragments of sandstone, believed to be of Cambrian age, occur in the Pleistocene glacial drift at Karstula. The microfossils contained in one pebble were analysed under the microscope and with the aid of scanning electronmicrographs. Four types were defined. They possibly represent blue-green algae...
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| Format: | Article |
| Language: | English |
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Geological Society of Finland
1974-06-01
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| Series: | Bulletin of the Geological Society of Finland |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume46/sgs_bt_046_1_pages_009_013.pdf |